Connoisseur’s Choice: Malachite Pseudomorphs after Azurite—Part 2: Milpillas, Mexico and Other Worldwide Localities

Q4 Earth and Planetary Sciences Rocks and Minerals Pub Date : 2022-10-05 DOI:10.1080/00357529.2022.2087150
P. Megaw, Evan A. Jones, B. Cairncross, Malcolm Southwood
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Abstract

Pseudomorphs of malachite after azurite are reasonably common in nature and are highly sought-after by mineral collectors; a tendency for sharp preservation of the original azurite habit coupled with strong, bright colors makes for attractive specimens. In Part 1 of this article, Southwood and Cairncross (2022) featured pseudomorphs of malachite after azurite from two classic localities, Bisbee, Arizona, and the Tsumeb mine in Namibia, and discussed aspects of the replacement mechanism on the scale of individual crystals. The featured locality for Part 2 (with an expanded author base) is the Milpillas mine, Sonora, Mexico, which, as noted previously, sets the modern benchmark for fine specimens of these replacements. Across the U.S. border in Arizona, a number of localities besides Bisbee have
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鉴赏家的选择:蓝铜矿后的孔雀石伪晶-第2部分:密皮拉斯,墨西哥和其他世界各地
孔雀石在天青石之后的假形态在自然界中相当常见,并且受到矿物收集者的高度追捧;强烈保留原始天青石习性的趋势,加上强烈明亮的颜色,使标本具有吸引力。在本文的第1部分中,Southwood和Cairncross(2022)介绍了来自亚利桑那州比斯比和纳米比亚Tsumeb矿这两个经典地区的孔雀石和天青石的假形态,并讨论了单个晶体规模上的置换机制。第2部分的特色地点(扩大了作者基础)是墨西哥索诺拉州的米尔皮拉斯矿,如前所述,该矿为这些替代品的精细标本树立了现代基准。在美国边境的亚利桑那州,除了比斯比之外,许多地方都有
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来源期刊
Rocks and Minerals
Rocks and Minerals Earth and Planetary Sciences-Geology
CiteScore
0.30
自引率
0.00%
发文量
85
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